Freezing rain event 1415 December 2005 Central South Carolina - PowerPoint PPT Presentation

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Freezing rain event 1415 December 2005 Central South Carolina

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Initially it appeared temperatures would be just warm enough for all rain. ... forecast 295K pressure (mb), 295K pressure advection (um/s, and wind (kt) valid ... – PowerPoint PPT presentation

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Title: Freezing rain event 1415 December 2005 Central South Carolina


1
Freezing rain event 14-15 December 2005Central
South Carolina
Tony Petrolito NWS Forecast Office Columbia SC
2
Introduction
  • Initially it appeared temperatures would be just
    warm enough for all rain. Cold dry high pressure
    to the north.
  • A light freezing rain event developed across the
    piedmont and north midlands after midnight 15
    December 2005.
  • Icing was confined to elevated surfaces (trees
    power lines). Soil temperatures well above
    freezing.

3
Introduction-Cont.
  • During the morning 14 December, WFO CAE
    forecasters determined (based on observational
    trends) that the numerical models and model
    output statistics (MOS) were incorrectly
    forecasting surface temperatures too warm and
    were also not accounting for dry air near the
    surface.
  • WFO CAE forecasters decided to issue a winter
    weather advisory for freezing rain for the
    northern portion of the county warning forecast
    area.

4
Synoptic overview
GFS 18-hr forecast 500mb geopotential heights
(m x 10), vorticity (s-1) and wind (kt) valid
1200 UTC 15 December 2005.
5
NCEP/HPC observed mean sea level pressure (mb)
and frontal analysis valid 1200 UTC 15 December
2005. (weak CAD with surface temperatures near
0oC across north central S.C.)
6
MSAS mean sea level pressure analysis (mb) and
METAR observations standard plot valid 1900 UTC
14 December 2005.

7
GFS 00-hr forecast precip water and precip water
observed plot valid 1200 UTC 14 December 2005.
8
NAM 00-hr forecast precip water and precip water
observed plot valid 1200 UTC 14 December 2005.
9
Laps sounding at CAE valid 1800 UTC 14 December
2005. note deep cold and dry layer below 600 mb.
The sounding saturated above 600 mb suggesting
extensive mid to high level clouds limiting solar
insolation during the afternoon.
10
ACARS sounding near CAE valid 1855 UTC 14
December 2005.
11
Mesoscale overview
MSAS mean sea level pressure (mb), surface
temperature oF and surface wind (kt) valid 2100
UTC 14 December 2005.
12
NAM 3-hr forecast mean sea level pressure (mb),
surface temperature oF and surface wind (kt)
valid 2100 UTC 14 December 2005.
13
CAE GFS MOS GUIDANCE 1200 UTC 14 December 2005
14
CAE NAM MOS GUIDANCE 1200 UTC 14 December 2005
15
NAM 24-hr forecast 295K pressure (mb), 295K
pressure advection (um/s, and wind (kt) valid
1200 UTC 15 December 2005. WFO CAE QPF forecasts
were in the 0.25 to 0.50 inch range for the 12-hr
period ending at 1200 UTC.
16
Fa1 if all the freezing takes place on elevated
surfaces Fa0.5 if freezing occurs on ground with
cold bare ground
icing (mm)0.05dTdP/Fa assuming adequate QPF
dTfreezing point depression (oC) dPdepth of
surface based sub-freezing layer(mb)
17
(No Transcript)
18
Winter weather advisory (issued at 1535 LST 14
Dec.)

19
Summary
  • Light to occasionally moderate freezing rain
    event developed after midnight 15 December.
  • With soil temperatures above 0oC, icing was
    confined to elevated surfaces. Local application
    based on CSTAR research suggested icing potential
    around 0.10 inches was possible. Spotter reports
    confirm icing accretion up to 0.10 inches on
    trees and power lines.
  • WFO CAE forecasters demonstrated excellent
    situational awareness by recognizing that the
    model forecasts of surface temperatures and dew
    points were not panning out in correspondence
    with observations.
  • It is important for forecasters to routinely
    compare model soundings with ACARS, Laps, and
    other observational data sets.
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